(Table 2) Radiocarbon dates of sediment cores obtained during Bio Hespérides cruise SVAIS and OGS Explora cruise EGLACOM between 2007-2008 ...

A high-resolution paleomagnetic and rock magnetic study has been carried out on sediment cores collected in glaciomarine silty-clay sequences from the continental shelf and slope of the southern Storfjorden trough-mouth fan, on the northwestern Barents Sea continental margin. The Storfjorden sedimen...

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Bibliographic Details
Main Authors: Sagnotti, Leonardo, Macrì, Patrizia, Lucchi, Renata G, Rebesco, Michele, Camerlenghi, Angelo
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
Event label
Latitude of event
Longitude of event
Elevation of event
DATE/TIME
Date/time end
Sample ID
DEPTH, sediment/rock
Age, dated material
Description
Method comment
Age, dated
Age, dated standard deviation
δ13C
Age, minimum/young
Age, maximum/old
Calendar age
Gravity corer
Piston corer
Age, 14C AMS
Age, 14C calibrated, CALIB 6.0 Reimer et al., 2009
EGLACOM
29HE20070802
OGS-Explora
Hespérides
International Polar Year 2007-2008 IPY
Barents Sea
International Polar Year
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.819543
https://doi.pangaea.de/10.1594/PANGAEA.819543
Description
Summary:A high-resolution paleomagnetic and rock magnetic study has been carried out on sediment cores collected in glaciomarine silty-clay sequences from the continental shelf and slope of the southern Storfjorden trough-mouth fan, on the northwestern Barents Sea continental margin. The Storfjorden sedimentary system was investigated during the SVAIS and EGLACOM cruises, when 10 gravity cores, with a variable length from 1.03 m to 6.41 m, were retrieved. Accelerator mass spectrometry (AMS) 14C analyses on 24 samples indicate that the cores span a time interval that includes the Holocene, the last deglaciation phase and in some cores the last glacial maximum. The sediments carry a well-defined characteristic remanent magnetization and have a valuable potential to reconstruct the paleosecular variation (PSV) of the geomagnetic field, including relative paleointensity (RPI) variations. The paleomagnetic data allow reconstruction of past dynamics and amplitude of the geomagnetic field variations at high northern ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...

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